Global temperature
HadCRUT5 · anomaly relative to 1850–1900
The Sun, volcanoes and ocean fluctuations affect climate. The question is whether they explain the long-term rise in global temperature. Here we compare their development over time and their assessed contributions to warming.
Choose a year. The markers move together across all charts. Each series keeps its own scale: similar-looking lines alone do not establish a cause.
HadCRUT5 · anomaly relative to 1850–1900
NOAA TSI · model-based annual mean at the top of the atmosphere
NOAA Niño 3.4 · mean of twelve monthly values
The solar series is a model-based NOAA climate dataset, not a satellite-only measurement. The Niño index describes sea-surface temperature in the tropical Pacific, not global temperature.
If more solar energy drove the long-term rise, its influence would have to increase accordingly over recent decades. The series shows solar-cycle fluctuations, but no matching long-term increase. Stronger sunlight would also warm the stratosphere; it has cooled.
NASA: the Sun and warmingMajor eruptions inject sulfate aerosols into the stratosphere. They reflect sunlight and can cool Earth for several years. This explains temporary deviations, but not a temperature trend rising over decades.
NASA GISS: volcanic aerosolsEl Niño and La Niña redistribute heat between the ocean and atmosphere. They strongly affect individual years. As internal variability, however, they do not add a lasting new source of energy to the climate system.
NOAA: Niño 3.4 dataChanges in Earth's orbit affect climate over many thousands of years. Their pace and current direction do not match the rapid temperature rise since the 20th century.
NASA: orbital cyclesThe IPCC assesses the change in global surface temperature in 2010–2019 relative to 1850–1900. The bars show uncertainty ranges in °C; they are not a time series through 2025.
The ranges describe uncertainty in each estimate. Observation and contributions are different quantities; their central values should not be read as exactly additive individual measurements.
IPCC AR6, Figure SPM.2Die Messreihen zeigen Schwankungen; die IPCC-Bewertung trennt deren Beiträge vom langfristigen menschlichen Einfluss. Der nächste Schritt prüft, wie dieser Einfluss unabhängig nachgewiesen wird.
Annual model-based solar irradiance · 1950–2025 · W/m²
Monthly values · aggregated to annual means · 1950–2025 · °C
Global temperature anomaly · 1950–2025 · 1850–1900 reference
Assessed contributions to warming in 2010–2019 relative to 1850–1900